FN Archimer Export Format
PT J
TI How does the Niger river warm coastal waters in the northern Gulf of Guinea?
BT 
AF Topé, G. D. A.
   Alory, G.
   Djakouré, S.
   Da-Allada, C.Y.
   Jouanno, J.
   Morvan, G.
AS 1:1,2;2:3;3:1,2;4:1,4,5;5:3;6:3;
FF 1:;2:;3:;4:;5:;6:;
C1 International Chair in Mathematical Physics and Application (ICMPA)-UNESCO Chair/University of Abomey Calavi (UAC), Cotonou, Benin
   Laboratory of Matter, Environment and Solar Energy Sciences, Félix Houphouët Boigny University in Abidjan, Abidjan, Côte d’Ivoire
   Centre National d’Etudes Spatiales CNES, Centre National de la Recherche Scientifique (CNRS), Institut de Recherche pour le Développement (IRD), Université Paul Sabatier (UPS), Laboratoire d’Etudes en Géophysique et Océanographie Spatiales (LEGOS), University of Toulouse, Toulouse, France
   Laboratoire de Géosciences, de l’Environnement et Applications (LaGEA)/Ecole Nationale Supérieure des Travaux Publics (ENSTP)/Université Nationale des Sciences, Technologies, Ingénierie et Mathématiques (UNSTIM), Abomey, Benin
   Laboratoire d’Hydrologie Marine et Côtiére (LHMC)/Institut de Recherche Halieutique et Océanologique du Benin (IRHOB), Cotonou, Benin
C2 UNIV ABOMEY CALAVI, BENIN
   UNIV FELIX HOUPHOUET BOIGNY, COTE IVOIRE
   CNRS, FRANCE
   UNIV ABOMEY CALAVI, BENIN
   IRHOB, BENIN
IN DOAJ
IF 3.7
TC 0
UR https://archimer.ifremer.fr/doc/00882/99410/109434.pdf
LA English
DT Article
CR PIRATA
DE ;coastal upwelling;Niger river plume;Gulf of Guinea;heat balance;tropical Atlantic
AB To highlight the processes by which the Niger River warms the coastal waters in the eastern part of the northern Gulf of Guinea upwelling, two simulations of the NEMO model at high resolution were used over the period 2010 - 2017. The first simulation is realistic while the second is a simulation in which the effects of the Niger River are not taken into account. The first step was to evaluate the outputs of the models, using satellite products and in situ observations. The average states of the Sea Surface Temperature, Salinity, Height, zonal current and vertical profiles of temperature and salinity showed the ability of the model to reproduce correctly the physical characteristics of the study area. The analysis of the heat balance terms of the two simulations showed that vertical diffusion and meridional advection processes are the causes of the warming induced by the Niger River. The stratification and vertical shear of the horizontal currents reveal that the river acts by inhibiting the upwelling of cold water induced by vertical diffusion. The river reinforces the stratification and prevents vertical shearing of horizontal currents at the bottom of the mixed layer. 
PY 2023
PD MAY
SO Frontiers In Marine Science
SN 2296-7745
PU Frontiers Media SA
VL 10
UT 000999512000001
DI 10.3389/fmars.2023.1187202
ID 99410
ER

EF